纳米秒的结构进化在震惊的共存中
Xiaokang Feng1,2, Shuning Pan3, Kento Katagiri4,5
1Center for High-Pressure Science and Technology Advanced Research, Beijing 100094, China.
Science advances
|April 25, 2025
概括
被冲击的coesite转化为新型的高压二氧化阶段,然后再回来. 这些复杂的相位过渡提供了对石撞击早期地球,月球和火星的矿物行为的新见解.
科学领域:
- 矿物物理 矿物物理
- 地质化学 地质化学
- 材料科学是一种材料科学.
背景情况:
- 矿物中冲击诱导的相变是理解冲击事件的关键.
- 之前对65GPa冲击的研究表明了复杂的高压阶段.
- 在极端压力下的行为,尤其是在化前的超热过程中,需要进一步调查.
研究的目的:
- 为了研究在激光驱动冲击下的coesite的时间依赖反应.
- 为了探索在高压下的复杂相位演变路径.
- 为了解外星撞击事件中发现的二氧化相提供见解.
主要方法:
- 激光驱动的冲击实验.
- 时间解析的X射线衍射 (XRD) 用于现场分析.
- 分子动力学模拟利用一种新的机器学习原子间潜力.
主要成果:
- 观察到一个短暂的密集超冷液体二氧化.
- 确定结晶成半无序的d-NiAs类型的二氧化.
- 有记录的变化为压力依赖的海弗或斯提索.
- 在释放压力时,揭示了反向转化为coesite,而不是石英.
结论:
- 被震惊的coesite表现出复杂的阶段进化路径.
- 观察到的相位和转变增强了对在极端冲击条件下的行为理解.
- 这些发现有助于解释石对陆地行星撞击记录中的高压二氧化相.
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